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Petroleum System in Deepwater Basins of the Northern South China Sea
Wu Shiguo1,2; Han Qinghua1,3; Ma Yubo1,3; Dong Dongdong1,3; Lue Fuliang4
2009-02-01
发表期刊JOURNAL OF EARTH SCIENCE
ISSN1674-487X
卷号20期号:1页码:124-135
文章类型Article
摘要The northern South China Sea margin has experienced a rifting stage and a post-rifting stage during the Cenozoic. In the rifting stage, the margin received lacustrine and shallow marine facies sediments. In the post-rifting thermal subsidence, the margin accumulated shallow marine facies and hemipelagic deposits, and the deepwater basins formed. Petroleum systems of deepwater setting have been imaged from seismic data and drill wells. Two kinds of source rocks including Paleogene lacustrine black shale and Oligocene-Early Miocene mudstone were developed in the deepwater basin of the South China Sea. The deepwater reservoirs are characterized by the deep sea channel rill, mass flow complexes and drowned reef carbonate platform. Profitable capping rocks on the top are mudstones with huge thickness in the post-rifting stage. Meanwhile, the faults developed during the rifting stage provide a migration path favourable for the formation of reservoirs. The analysis of seismic and drilling data suggests that the joint structural and stratigraphic traps could form giant hydrocarbon fields and hydrocarbon reservoirs including syn-rifting graben subaqueous delta, deepwater submarine fan sandstone and reef carbonate reservoirs.; The northern South China Sea margin has experienced a rifting stage and a post-rifting stage during the Cenozoic. In the rifting stage, the margin received lacustrine and shallow marine facies sediments. In the post-rifting thermal subsidence, the margin accumulated shallow marine facies and hemipelagic deposits, and the deepwater basins formed. Petroleum systems of deepwater setting have been imaged from seismic data and drill wells. Two kinds of source rocks including Paleogene lacustrine black shale and Oligocene-Early Miocene mudstone were developed in the deepwater basin of the South China Sea. The deepwater reservoirs are characterized by the deep sea channel rill, mass flow complexes and drowned reef carbonate platform. Profitable capping rocks on the top are mudstones with huge thickness in the post-rifting stage. Meanwhile, the faults developed during the rifting stage provide a migration path favourable for the formation of reservoirs. The analysis of seismic and drilling data suggests that the joint structural and stratigraphic traps could form giant hydrocarbon fields and hydrocarbon reservoirs including syn-rifting graben subaqueous delta, deepwater submarine fan sandstone and reef carbonate reservoirs.
关键词Deepwater Reservoir Source Rock Petroleum System Northern South China Sea
学科领域Geosciences, Multidisciplinary
DOI10.1007/s12583-009-0014-3
收录类别SCI
语种英语
WOS记录号WOS:000264753800013
引用统计
被引频次:23[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/3712
专题海洋地质与环境重点实验室
作者单位1.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China
2.China Univ Petr, Coll Georesource & Informat, Qingdao 266555, Peoples R China
3.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
4.PetroChina Hangzhou Inst Geol, Hangzhou 310023, Zhejiang, Peoples R China
第一作者单位中国科学院海洋研究所
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GB/T 7714
Wu Shiguo,Han Qinghua,Ma Yubo,et al. Petroleum System in Deepwater Basins of the Northern South China Sea[J]. JOURNAL OF EARTH SCIENCE,2009,20(1):124-135.
APA Wu Shiguo,Han Qinghua,Ma Yubo,Dong Dongdong,&Lue Fuliang.(2009).Petroleum System in Deepwater Basins of the Northern South China Sea.JOURNAL OF EARTH SCIENCE,20(1),124-135.
MLA Wu Shiguo,et al."Petroleum System in Deepwater Basins of the Northern South China Sea".JOURNAL OF EARTH SCIENCE 20.1(2009):124-135.
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